ClimateSearch

Kakogawachō-honmachi, Hyōgo

Japan · 272k people · 7 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high47°F (8°C)48°F (9°C)54°F (12°C)62°F (17°C)70°F (21°C)76°F (24°C)82°F (28°C)85°F (29°C)79°F (26°C)70°F (21°C)61°F (16°C)51°F (11°C)
Average low36°F (2°C)36°F (2°C)40°F (5°C)48°F (9°C)57°F (14°C)65°F (19°C)74°F (23°C)76°F (24°C)69°F (21°C)59°F (15°C)49°F (9°C)40°F (4°C)
Dew point31°F (0°C)32°F (0°C)37°F (3°C)47°F (8°C)56°F (14°C)65°F (18°C)73°F (23°C)74°F (23°C)66°F (19°C)56°F (13°C)46°F (8°C)36°F (2°C)
Rainfall1.9 in (49 mm)2.4 in (61 mm)4 in (102 mm)4.7 in (119 mm)5.5 in (140 mm)7.1 in (181 mm)7.4 in (188 mm)4.5 in (115 mm)7.6 in (193 mm)5.9 in (150 mm)3 in (76 mm)2.4 in (62 mm)
Rainy days6710101013141113977
Snowfall0.3 in (0.7 cm)1 in (2.6 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.1 in (0.3 cm)
Sunshine248 h237 h274 h274 h304 h263 h304 h334 h269 h257 h236 h244 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+2.3°F (+1.3°C)

Models range from +1.7°F (+1.0°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.1°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.3°F (+1.3°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.